The role of phosphorus in rhyolitic liquids as determined from the homogeneous iron redox equilibrium

The role of phosphorus in rhyolitic liquids as determined from the homogeneous iron redox equilibrium

The redox ratio of iron is used as an indicator of solution properties of silicate liquids. The homogeneous iron redox equilibrium is employed to determine the role of phosphorus in rhyolitic liquids.

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Bibliographische Detailangaben
Veröffentlicht in:Contributions to mineralogy and petrology 1993-03, Vol.113 (3), p.424-435
Hauptverfasser: GWINN, Rosa, HESS, Paul C
Format: Artikel
Sprache:eng
Schlagworte:
Chemistry
Crystalline rocks
Earth sciences
Earth, ocean, space
Exact sciences and technology
Experimental petrology
Geology
Iron
Mineralogy
Minerals
Petrology
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Zusammenfassung:The redox ratio of iron is used as an indicator of solution properties of silicate liquids. The homogeneous iron redox equilibrium is employed to determine the role of phosphorus in rhyolitic liquids.
ISSN:0010-7999
1432-0967
DOI:10.1007/BF00286932